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Titlebook: Impact Tectonics; Christian Koeberl,Herbert Henkel Book 2005 Springer-Verlag Berlin Heidelberg 2005 Deformation.Dike.Economic Ecology.Frac

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发表于 2025-3-21 17:38:46 | 显示全部楼层 |阅读模式
书目名称Impact Tectonics
编辑Christian Koeberl,Herbert Henkel
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概述Current knowledge of impact tectonics, geological and geophysical investigations of terrestrial impact structures, and suggested new impact structures.Includes supplementary material:
丛书名称Impact Studies
图书封面Titlebook: Impact Tectonics;  Christian Koeberl,Herbert Henkel Book 2005 Springer-Verlag Berlin Heidelberg 2005 Deformation.Dike.Economic Ecology.Frac
描述This volume is the latest of eight books as a result of the activities of the scientific program on ”The Response of the Earth System to Impact Processes” (IMPACT) of the European Science Foundation (ESF). The ESF is the European association of national funding organisations of fundamental research, with more than 60 member organisations from more than 20 countries. One of the main goals of ESF is to bring European scientists together to work on topics of common interest. The ESF IMPACT program deals with all aspect of impact research, mainly through the organisation of workshops, exchange program, short course, and related activities. An important aspect of the program is to stimulate interdisciplinary and international research. Impacts of asteroids or comets on the earth surface have played an important role in the evolution of the planet. The ESF IMPACT program is an interdisciplinary program aimed at understanding impact processes and their effect on the earth system, including environmental, biological, and geological changes, and consequences for the biodiversity of ecosystems. The key goal of the program, to comprehend the processes that are responsible for these interactio
出版日期Book 2005
关键词Deformation; Dike; Economic Ecology; Fracture Patterns; Impact Mechanisms; Pseudotachylite Formation; Stru
版次1
doihttps://doi.org/10.1007/3-540-27548-7
isbn_softcover978-3-642-42131-0
isbn_ebook978-3-540-27548-0Series ISSN 1612-8338
issn_series 1612-8338
copyrightSpringer-Verlag Berlin Heidelberg 2005
The information of publication is updating

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The Mechanics of Pseudotachylite Formation in Impact Eventsf a large meteorite impact. The prevailing opinion among many geologists is that pseudotachylites are formed by friction melting of rocks and/or shearing associated with differential shock compression of adjacent rock types. Several physical studies of friction melting have shown that, in theory, sm
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The Preliminary Analysis of Polygonal Impact Craters within Greater Hellas Region, Mars on all kinds of celestial bodies that have fractured rigid crusts. They are also found on the Earth (e.g., Meteor Crater, Söderfjärden). Polygonal craters are thought to have been formed by two possible mechanisms. Simple polygonal craters, such as the square-shaped Meteor Crater, result when the e
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Settings of Meteorite Impact Structures in the Svecofennian Crustal Domain Together with younger (1.5 – 1.8 Ga) transition zones it occupies an area of ~1.56 × 10. km.. The domain unites shield and platform areas including the submerged Baltic Sea. It includes 22 confirmed, 6 possible, and tens of supposed impact structures that survived recurrent erosional epochs during
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Geophysical Investigations of the Siljan Impact Structure — A Short Reviewons indicate an age of 377 Ma. The bedrock geology of the region has recently been re-mapped by the Geological Survey of Sweden in the scale of 1:50 000. There is now complete coverage with airborne geophysics. New maps of the geophysical data have been prepared for this review. In connection with t
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Mjølnir Crater as a Result of Oblique Impact: Asymmetry Evidence Constrains Impact Direction and Ang5°) angle from the horizontal. This is substantiated by several diagnostic structural and geophysical signatures related to obliquity and revealed through detailed re-assessment of Mjølnir’s well-established structure, morphology, and gravity and seismic velocity anomalies. The diagnostic signatures
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